HAVÍŘ, Josef and Zdeněk STRÁNÍK. Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia). Geologica Carpathica. Bratislava: SAV, 2003, vol. 54, No 6, p. 409-416. ISSN 1335-0552.
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Basic information
Original name Orientations of paleostresses in the Jurassic limestones on the front of the West Carpathian flysch nappes (Pavlov Hills, South Moravia)
Authors HAVÍŘ, Josef and Zdeněk STRÁNÍK.
Edition Geologica Carpathica, Bratislava, SAV, 2003, 1335-0552.
Other information
Original language English
Type of outcome Article in a journal
Field of Study 10500 1.5. Earth and related environmental sciences
Country of publisher Slovakia
Confidentiality degree is not subject to a state or trade secret
Impact factor Impact factor: 0.397
Organization unit Faculty of Science
UT WoS 000189225600006
Keywords in English Neogene; Outer Western Carpathians; Waschberg-Ždánice Belt; paleostresses
Tags Neogene, Outer Western Carpathians, paleostresses, Waschberg-Ždánice Belt
Changed by Changed by: Mgr. Josef Havíř, Dr., učo 2127. Changed: 10/2/2004 14:01.
Abstract
The paleostress analysis was applied at 16 sites in the Mesozoic limestones, which are tectonically incorporate into the Cretaceous and the Paleogene strata on the front of the Western Carpathian Flysch nappes (South Moravia, Czech Republic). 25 solutions were obtained. These solutions can be divided into two groups. First group represents the paleostress field with predominantly NW-SE compression and NE-SW extension connected with the Early Neogene movements of the Ždánice nappe. The azimuth of eigenvector of acceptable compression axes varies from 97 up to 167. This variability can be explained by rotation of individual tectonic slices of the Ždánice nappe during the movement this nappe. The different tectonic scales rotated probably in different sense (anticlockwise rotation in the case of some scales, clockwise rotation in the case of other scales). Second group of solutions represents the paleostress field with NE-SW compression and NW-SE extension.
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